Reverse fault
When rocks beneath the Earth's surface undergo stress, they can deform and eventually break. This can result in the formation of faults and earthquakes, as well as the folding and shifting of rock layers. Over time, continued stress can lead to the movement of tectonic plates and the creation of mountain ranges.
The stress that squeezes rock until it folds or breaks is called compressional stress. This type of stress occurs when forces push together in opposite directions, causing rocks to deform under pressure.
erosion happens
Because of friction and the rigidity of the rock, the rocks cannot glide or flow past each other. Rather, stress builds up in rocks and when it reaches a level that exceeds the strain threshold, the accumulated potential energy is dissipated by the release of strain, which is focused into a plane along which relative motion is accommodated-the fault.
Sediment builds up over time and expands. Probably like a huge rock or a giant elephant.
It could help you relax and relieve stress.
Ductile deformation is when rock is given enough stress to break. If the stress is less, it will bend but not break.
I found that folding happens
Elastic rebound. This phenomenon occurs when stress builds up in a rock mass and causes it to deform, then suddenly release that stress by rebounding to its original shape. Elastic rebound is often associated with earthquakes and fault movements.
When rock layers are folded, a geological fold happens. These folds form under various conditions such as stress, hydrostatic pressure, pore pressure, and temperature gradient.
Yes, stress can build up along fault lines where rocks snag and remain locked. This stress can accumulate over time until it is released in the form of an earthquake when the built-up energy exceeds the strength of the rocks holding the fault together.